Two novel, designated strains 29W222T and 2943T, were isolated from the marine sediment from Aoshan Bay, Jimo, PR China. Growth was observed at pH 6.0–8.5 (optimum, pH 7.5) for strain 29W222T, and pH 5.5–8.5 (pH 7.0) for strain 2943T. Both strains displayed growth in 0.5–6 % NaCl with an optimum at 1 % for 29W222T; 0.5 % for 2943T. Both strains grew optimally at 33 °C. The results of phylogenetic analyses based on 16S rRNA gene sequences indicated that 29W222T and 2943T represented members of the genus Fulvivirga and strain 29W222T was most closely related to Fulvivirga kasyanovii KMM 6220T (97.9 % sequence similarity) and Fulvivirga imtechensis AK7T (95.0 %), and 2943T to Fulvivirga imtechensis AK7T (95.7 %) and Fulvivirga kasyanovii KMM 6220T (94.8 %). The genomic DNA G+C contents of 29W222T and 2943T were 39.9 and 37.7 mol%, respectively. The results of chemotaxonomic analysis indicated that the sole respiratory quinone was menaquinone 7 (MK-7), and the major fatty acid was iso-C15 : 0 for both strains. Average nucleotide identity and average amino acid identity values between strain 29W222T and Fulvivirga kasyanovii KMM 6220T were 78.9 and 83.6 %, respectively; the corresponding values between 2943T and Fulvivirga imtechensis AK7T were 69.8 and 63.6 %, respectively. Therefore, strains 29W222T and 2943T represent to two novel species of the genus Fulvivirga , for which the names Fulvivirga marina sp. nov. (29W222T=KCTC 62848T=MCCC 1K05194T) and Fulvivirga sediminis sp. nov. (2943T=KCTC 62847T= MCCC 1K05144T) are proposed, respectively.
Magnetotactic bacteria (MTB) are a group of prokaryotes that, despite their high morphological, phylogenetic, and ecological diversity, share a common capability of forming intracellular nanocrystals of magnetite (Fe3O4) or greigite (Fe3S4), called magnetosomes, and swimming along geomagnetic field lines in a process called magnetotaxis. In this study, we investigated the MTB diversity within the intertidal sediments near Xiaoshi Island (Weihai) in the North Yellow Sea using a combination of molecular ecology techniques and transmission electron microscopy (TEM). The combination of restriction fragment length polymorphism (RFLP) analysis and 16S rRNA gene sequencing revealed seven new MTB genera affiliated with the Alphaproteobacteria class. Fluorescencein situhybridization (FISH) analyses suggested that one magnetotactic coccus (designated as WHI-2) is the dominant species. TEM observations and energy dispersive X-ray analyses revealed that MTB cells mainly form magnetite magnetosomes that are organized into two chains of magnetosomes composed of e-prismatic magnetite crystals. This finding suggests the adaptation of a magnetotactic bacterial population to the marine tide. This is the first report of magnetotactic bacteria near Xiaoshi Island, which should be useful for studies of biogeochemical cycling and the geohistory of this area.
Erythrina corallodendron L., a kind of landscape tree, has long been used as a traditional medicine. In this study, the composition of essential oil extracted from the leaves was analysed by GC-MS (gas chromatograph-mass spectrometer), with linalool identified as the main compound. Its cytotoxicity against MDA-MB-231, MCF-7 and HMLE cells was examined by MTT and cloning assays. Transwell and wound-healing assays were used to examine the inhibition of migration and invasion. Western blot, qRT-PCR and immunofluorescence staining were used to measure the mRNA and protein expression of factors related to EMT (snail, slug, E-cadherin, N-cadherin and vimentin). The essential oil of Erythrina corallodendron leaves was found to inhibit the proliferation, migration and invasion of breast cancer cells in a dose-dependent manner. The findings of this study suggest that the essential oil of E. corallodendron leaves may merit further investigation as a potential clinical or adjuvant drug for treating breast cancer migration and invasion.
A time series of satellite data on Chlorophyll- a concentration (Chl- a ) that used ocean color was studied to determine mechanisms of phytoplankton variation in recent decade in the Yellow Sea, China during 2003–2015. The variability patterns on seasonal and inter-annual oscillation periods were confirmed using the Empirical Orthogonal Function (EOF), and Morlet wavelet transform analyses, respectively. The first EOF mode for Chl- a was dominated by obvious spring and fall blooms in a spatial pattern that was related to the strong mixing of the water masses from the Yellow Sea Cold Warm Mass (YSCWM) and the Yellow Sea Warm Current (YSWC) in winter. The second EOF mode for Chl- a showed an opposite spatial pattern between the northern and southern regions. The temporal coefficient showed differences in the timing of blooms. On an inter-annual scale, Chl- a indicated variation at periods of 2–4 years during 2003–2015. Chl- a showed a significantly negative correlation with the sea surface temperature (r = -0.21, p<0.01), with time lags of 4 months (Chl- a ahead). Chl- a was coupled with El Niño Southern Oscillation (ENSO) events, with a positive correlation (r = 0.46, p<0.01) at a lag of 3–5 months (ENSO ahead). The present study demonstrated that the variation in phytoplankton biomass was controlled primarily by water mass seasonally, and it was influenced by ENSO events on an inter-annual scale.
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